The Oxfordian carbonate platform of Lorraine:: evidences for an opening toward the Germanic Sea

被引：8

作者：

Carpentier, C

Lathuilière, B

Ferry, S

机构：

[1] Univ Nancy 1, Lab G2R, UMR 7566, F-54506 Vandoeuvre Les Nancy, France

[2] Univ Lyon 1, UMR 5125, F-69622 Villeurbanne, France

来源：

COMPTES RENDUS GEOSCIENCE | 2004年 / 336卷 / 01期

关键词：

Middle Oxfordian; Lorraine; Paris Basin; carbonate platform; coral breccias; hurricanes palaeogeography; France;

D O I：

10.1016/j.crte.2003.10.018

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The study of sedimentary facies in the quarry of Dompcevrin (Middle Oxfordian) located northwestward of St-Mihiel (Meuse department) provides evidences of high-energy depositional conditions. The occurrence of beaches associated with hurricane coral breccias containing megaclasts is characteristic of platform edge environments. The open sea was located northeastward, in the direction of Germany, as it is indicated by the direction of progradation of beaches. It is concluded that the Oxfordian carbonate platform of Lorraine was opened to the northeast toward the Germanic Sea during the Middle Oxfordian. (C) 2003 Academie des sciences. Publie par Elsevier SAS. Tous droits reserves.

引用

页码：59 / 66

页数：8

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